Paleoproterozoic Era
Quick Summary
The Paleoproterozoic Era is a division of geologic time within the Proterozoic Eon, spanning from approximately 2.5 billion to 1.6 billion years ago. This era is characterized by significant geological events, including the development of plate tectonics and the formation of large continental blocks.1234
A key environmental development during this period was the oxygenation of Earth's atmosphere. Evidence suggests that by the beginning of the Paleoproterozoic, oxygen levels had risen sufficiently to support oxidative weathering, as indicated by the presence of hematite-rich soils and red beds. The formation of banded-iron formations (BIFs) also provides insights into the changing chemistry of the oceans and atmosphere during this time.5
Correlating rock strata from the Paleoproterozoic is challenging due to the scarcity of fossils. Instead, geochronology, particularly zircon dating, is crucial for comparing and dating rocks across different regions and continents.67
- Precambrian - Major subdivisions of the Precambrian System
- Precambrian - Oxygenation of the atmosphere
- Precambrian - Proterozoic plate movements
- Precambrian - Archean crustal growth
- era
- Tertiary Period - Correlation of Tertiary strata
- Precambrian - Correlation of Precambrian strata
- dating - Double uranium-lead chronometers
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